Abstract

The discovery of the Carnian Pluvial Episode arose through a chance conversation bringing together two seemingly unrelated strands of research: the extinction of some Triassic crinoids and the stratigraphy of the non-marine Mercia Mudstone Group. Investigations revealed a hitherto unrecognised period of climate change seemingly linked to a largely overlooked episode of biotic turnover. Ignored for more than a decade, an upsurge of interest in recent years has validated our original findings and answered some of the key questions concerning its extent and ultimate cause.

You do not currently have access to this article.